广西平乐县小王家铜矿地质特征及找矿标志  

THE GEOLOGICAL FEATURE AND PROSPECTING CRITERIA OF XIAOWANGJIA CU DEPOSIT IN PINGLE,GUANGXI

作　　者：何智聪[1] 欧远新 卫小彦 莫次生 

机构地区：[1]广西平乐县国土资源局,广西桂林542400 [2]广西壮族自治区二七一地质队,广西桂林541100

出　　处：《云南地质》2015年第1期75-78,共4页Yunnan Geology

摘　　要：平乐县小王家铜矿区处于华南准地台之桂中—桂东台陷中的大瑶山凸起中段北缘。矿体产于断裂破碎带中,且该组含矿断裂又被泥盆系不整合覆盖,小王家铜矿无疑为加里东期构造运动的产物。该铜矿床属中低温热液充填脉型铜矿床。Xiaowangjia Cn orefield of Pingle is in the N margin of middle section of Dayaoshan rise in Guizhong-Guidong platform sag of S China paraplafform. The ore body is in the fracture zone. And the ore-bearing faule is covered unconformably by D, which is formed doubtlessly by Caledonian movement. It is a middle-low T hydrothermal filling veined Cu deposit.

关 键 词：加里东期断裂控矿 热液充填 广西平乐县小王家 

分 类 号：P618.41[天文地球—矿床学]